data
Metcalfe, B., Lougheed, B.C., Waelbroeck, C., and Roche, D.M. (submitted). On the validity of foraminifera-based ENSO reconstructions.
Pracht, H., Metcalfe, B., and Peeters, F.J.C., (2019). Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth. Biogeosciences, 16 (2), 643-661
Metcalfe, B., Feldmeijer, W., de Vringer-Picon, M., Brummer, G.-J.A., Peeters, F.J.C. and Ganssen, G.M. (2015) Late Pleistocene GlacialāInterglacial related shell size isotope variability in planktonic foraminifera as a function of local hydrology. Biogeosciences 12 (15), 4781-4807. DOI: 10.5194/bg-12-4781-2015
Feldmeijer, W., Metcalfe, B. Scussolini, P., Arthur, K., (2013) The effect of chemical pretreatment of sediment upon foraminiferalābased proxies. Geochemistry, Geophysics, Geosystems 14 (10), 3996-4014. DOI:10.1002/ggge.20233
FAME Model output from a single time step of a ~50 year model run. Each panel represents a single species oxygen isotope values.
Predicted depth habitats from oxygen isotope values (Pracht et al., 2019).
Single shell oxygen isotope data down core for different size fractions (Metcalfe et al., 2015).
The impact of the pH with time, of the solution of deep-sea sediment and chemical pretreatment (Feldmeijer et al., 2013).